User:ZKW23/Albtrauf



The term „Albtrauf“ (Alp escarpments) refers to the northwest facing escarpment of the Swabian Alps which is situated in Baden-Württemberg and Bavaria. It is the most distinctive stepped slope within the alpine region of the South German Scarplands, leading roughly from the southwest to the northeast.

The Albtrauf has its geological extension in the northeast, in the stepped slopes of the Franconian Jura and in the southwest and west among the Jurassic-era stepped slopes of the Baaralb, Hegaualb, Randen, Klettgau, Aargau as well as the Table Jura stretches from the city of Basel to the Ajoie and the French Scarplands.

In geology and geomorphology, however, the term “Trauf” merely describes the brink of the stepped slopes where various stepped surfaces meet (which is not developed in hipped steps).

Geography


Like the entirety of the Swabian Alps, the Albtrauf leads from the southwest to the northeast, approximately following the line of Donaueschingen–Lemberg–Balingen–Reutlingen–Kirchheim unter Teck–Gingen an der Fils–Unterkochen. On a closer look it is markedly interrupted by many deeply eroded valleys.

The protruding inliers and outliers (German: Zeugenberge) support famous castles, which are visible from a great distance, such as the Hohenzollern Castle, the Hohenneuffen Castle and the Teck Castle. Major traffic routes leading from the alpine foothills to the Albtrauf are known as the Alb ascension (German: Albaufstieg), the best known of them being the Geislinger Steige.

Geology
The Albtrauf is made up of an upper rock layer of the Brown Jurassic and lower and middle layers of the White Jurassic. The harder layers of the Brown Jurassic act as the foundation of this bed and so form the highest, often weakly developed layer of the Alpine foothills. The Brown Jurassic differs regionally: Sandflaserschichten (Quenstedtsche Gliederung B β) in the eastern Alps, Blaukalke (B γ) in the mid Alps, oolithische Kalkmergel (B δ) in the western Alps. The lower section of the stepped slope are made up of the claystone layers of the Brown Jurassic, stretching to the Ornatenton Formation which ends this section. The equally soft Kalkmergel (W α) follows as the first layer of the White Jurassic. Hard limestone is a viable layer-forming component in the W β (as reef limestone in the western Alps, otherwise as the mural Wohlgeschichtete Kalk Formation), as well as in the W δ (reef limestone is found across the whole region, but especially in the young layers). In between these is a marl complex.

Geomorphology

The intermediate inclination of the Albtrauf amounts to roughly 35 degrees. The Albtrauf reaches an average height of nearly 400 m in the region of the Erms valley and near Balingen. The edge of the slope is at approximately 1000 m.a.s.l. (metres above sea level) NHL (German: Normalhöhennull, English: standard elevation zero) in the southwest and at approximately 650 m.a.s.l. NHN in the northeast.

In the east of the alps and in parts of the middle alps (up to Bad Urach) W ß does not appear as step formatter, but at best as escarpment in the slope which climbs up to the W δ at a stroke. W ß and W δ levels, with the latter being about 100 m high, are distinctly pronounced from Reutlingen to Mössingen. Further to the west the W ß forms both the front of the Albtrauf and an adjoining dip slope, which is several kilometres broad. Moreover, the W δ step, which includes inliers and outliers located on the outskirts such as Kornbühl, is retrogressing.

The Albtrauf retrogresses (as it has done for millions of years) on average every year a few millimetres to the southeast due to retrogressive erosion, which explains the sinuate progression and the embayment. Similarly, landslides and rockfalls are responsible for this process. The ensemble of relief features includes cuestas, front side valleys, rock ledges, spurs and inliers. From northeast to southwest the Ipf, the Hohenstaufen, Achalm and Hohenzollern (Zoller) are counted among the most famous inliers and outliers without a dip slope. Kaltes Feld, Michelsberg, Farrenberg, the plateau of Burgfelden (Böllat-Heersberg) and Plettenberg rank among the most impressive inliers and outliers with a dip slope.

Miscellaneous
The vegetation consists mainly of beech wood forest. Juniper heathland, typical of the high plains of the Swabian Alps, can also be found in scattered locations, such as on Jusi, and are generally under conservation. Slow-growing oaks grow on the rocky outcrops. {{citation|surname1=A.Kerner,M.Geisel|editor-surname1= FVA|title=Waldkartierung. Forstliche Versuchs- und Forschungsanstalt Baden-Württemberg (FVA)|publication-place=Freiburg|at=p. 73|date=2010-08-30|language=German Spruce and fir forest can also be found in the Hohen Schwabenalb (high Swabian Alps) as a result of forestry untypical for the area. White outcrops of reef limestone protruding out of the forest all around are also characteristic. The Albtrauf was poetically dubbed “Blue Wall” by Eduard Mörike, owing to the pale blue shimmer that appears when it is viewed from a distance. The Schwäbische-Alb-Nordrand-Weg (Hauptwanderweg 1, HW 1), a hiking trail maintained by the Schwäbischen Albverein (Swabian Jura Association), provides access to the Albtrauf and leads from Donauwörth to Tuttlingen.

Literature

 * Reiner Enkelmann, Dieter Ruoff, Wolfgang Wohnhas: Der Albtrauf. Natur und Kultur zwischen Ries und Randen. Silberburg-Verlag, Tübingen und Lahr/Schwarzwald 2010. ISBN 978-3-87407-892-4
 * Otto F. Geyer und Manfred P. Gwinner: Einführung in die Geologie von Baden-Württemberg. Stuttgart 1964, S. 60 ff. und S. 148 ff.
 * Klaus Eberhard Bleich: Das Alter des Albtraufs. In: Jahreshefte des Vereins für vaterländische Naturkunde in Württemberg 115, Stuttgart, 1. November 1960, S. 39–92